Martin M. Miles' photos with the keyword: Saint Géry-Vers
Saint Géry-Vers - Divona Aqueduct
| 03 Nov 2025 |
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The Divona Aqueduct is one of the oldest aqueducts in France. It dates back to the early first century AD and supplied the Gallo-Roman town of Divona Cadurcorum (= Cahors). Water was channeled from a spring in the Vers Valley over a distance of 31.6 kilometers to the local baths. The aqueduct's canal is carved into the rock over long distances and further built as a brick canal. It was probably in use until the 4th or even 5th century AD.
The average gradient is 1.15 m per km (0.11%)
Saint Géry-Vers - Divona Aqueduct
| 03 Nov 2025 |
|
|
The Divona Aqueduct is one of the oldest aqueducts in France. It dates back to the early first century AD and supplied the Gallo-Roman town of Divona Cadurcorum (= Cahors). Water was channeled from a spring in the Vers Valley over a distance of 31.6 kilometers to the local baths. The aqueduct's canal is carved into the rock over long distances and further built as a brick canal. It was probably in use until the 4th or even 5th century AD.
The average gradient is 1.15 m per km (0.11%)
Saint Géry-Vers - Divona Aqueduct
| 02 Nov 2025 |
|
|
|
The Divona Aqueduct is one of the oldest aqueducts in France. It dates back to the early first century AD and supplied the Gallo-Roman town of Divona Cadurcorum (= Cahors). Water was channeled from a spring in the Vers Valley over a distance of 31.6 kilometers to the local baths. The aqueduct's canal is carved into the rock over long distances and further built as a brick canal. It was probably in use until the 4th or even 5th century AD.
The average gradient is 1.15 m per km (0.11%)
Saint Géry-Vers - Divona Aqueduct
| 02 Nov 2025 |
|
|
The Divona Aqueduct is one of the oldest aqueducts in France. It dates back to the early first century AD and supplied the Gallo-Roman town of Divona Cadurcorum (= Cahors). Water was channeled from a spring in the Vers Valley over a distance of 31.6 kilometers to the local baths. The aqueduct's canal is carved into the rock over long distances and further built as a brick canal. It was probably in use until the 4th or even 5th century AD.
The average gradient is 1.15 m per km (0.11%)
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